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    MASCON—A Mass Consistent Atmospheric Flux Model for Regions with Complex Terrain

    Source: Journal of Applied Meteorology:;1978:;volume( 017 ):;issue: 003::page 241
    Author:
    Dickerson, Marvin H.
    DOI: 10.1175/1520-0450(1978)017<0241:MMCAFM>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: MASCON was developed to provide air pollution models for the San Francisco Bay Area with mass consistent meteorological input data. Measurements of inversion base heights above topography and mean winds within the mixed layer calculated from surface observations of wind speed and direction were used as input data for the model. Variational calculus techniques were used to adjust the observed horizontal fluxes so they satisfied the continuity equation. In cases where air within the elevated inversion was entrained into the mixed layer, we used a parameterization of the vertical velocity. This model can also accept solid boundaries in the interior of the grid simulating conditions in the Bay Area where the base of the inversion is below some of the topographic features. This results in the horizontal flow fields being forced around these obstacles.
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      MASCON—A Mass Consistent Atmospheric Flux Model for Regions with Complex Terrain

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4232882
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    • Journal of Applied Meteorology

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    contributor authorDickerson, Marvin H.
    date accessioned2017-06-09T17:39:19Z
    date available2017-06-09T17:39:19Z
    date copyright1978/03/01
    date issued1978
    identifier issn0021-8952
    identifier otherams-9399.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4232882
    description abstractMASCON was developed to provide air pollution models for the San Francisco Bay Area with mass consistent meteorological input data. Measurements of inversion base heights above topography and mean winds within the mixed layer calculated from surface observations of wind speed and direction were used as input data for the model. Variational calculus techniques were used to adjust the observed horizontal fluxes so they satisfied the continuity equation. In cases where air within the elevated inversion was entrained into the mixed layer, we used a parameterization of the vertical velocity. This model can also accept solid boundaries in the interior of the grid simulating conditions in the Bay Area where the base of the inversion is below some of the topographic features. This results in the horizontal flow fields being forced around these obstacles.
    publisherAmerican Meteorological Society
    titleMASCON—A Mass Consistent Atmospheric Flux Model for Regions with Complex Terrain
    typeJournal Paper
    journal volume17
    journal issue3
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1978)017<0241:MMCAFM>2.0.CO;2
    journal fristpage241
    journal lastpage253
    treeJournal of Applied Meteorology:;1978:;volume( 017 ):;issue: 003
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian